Soil and Unsaturated Flow

External reference: https://openalex.org/T10716

  1. Water Adsorption of Non-Saline and Salt-Affected Clay
    Water vapor adsorption in salt-affected clays varies with humidity, with salinity enhancing uptake at high relative humidity through capillary condensation.
  2. Temporal linearization can bias root water uptake estimates
    Temporal linearization approximations for estimating root water uptake from soil-water flux gradients fail under dynamic field conditions, introducing substantial systematic errors in hydraulic.
  3. Freeze–thaw reshapes water, salt, and heat in saline farmland soil
    Freeze-thaw driven water-salt redistribution in saline farmland soils: quantified hydrothermal parameters and coupled migration mechanisms from field-laboratory verification.